Preface / Introduction / Energy partitioning during an earthquake / Rachel E. Abercrombie, Art McGarr, Giulio Di Toro, and Hiroo Kanamori -- Rachel E. Abercrombie, Art McGarr, Hiroo Kanamori, and Giulio Di Toro -- Hiroo Kanamori and Luis Rivera. A brief review of techniques used to estimate radiated seismic energy / The scaling of seismic energy with moment: simple models compared with observations / An overview of the global variability in radiated energy and apparent stress / The radiated energy of the 2004 Sumatra-Andaman earthquake / Uncertainties in earthquake source spectrum estimation using Empirical Green Functions / Source paramenters determined from microearthquakes in an underground ore mine / Source scaling relationships of microearthquakes at Parkfield, CA, determined using the SAFOD Pilot Hole seismic array / Effects of methods of attenuation correction on source parameter determination / Anupama Venkataraman, John Boatwright, and Gregory C. Beroza -- William R. Walter, Kevin Mayeda, Rengin Gok, and Abraham Hofstetter -- George L. Choy, Art McGarr, Stephen H. Kirby, and John Boatwright -- Hiroo Kanamori -- Germán A. Prieto, Robert L. Parker, Frank L. Vernon, Peter M. Shearer, and David J. Thomson -- Volker Oye, Michael Roth, and Hilmar Bungum -- Kazutoshi Imanishi and William L. Ellsworth -- Eleanor Sonley and Rachel E. Abercrombie. Section I: the measure of radiated energy and its behavior Inferring earthquake source properties from laboratory observations and the scope of lab contributions to source physics / Relating high-velocity rock-friction experiments to coseismic slip in the presence of melts / Shear resistance reduction due to vibration in simulated fault gouge / Quantitative characterization of permeability reduction associated with compactive cataclastic flow / N.M. Beeler -- Giulio Di Toro, Takehiro Hirose, Stefan Nielsen, and Toshihiko Shimamoto -- Takane Hori, Hide Sakaguchi, Naoto Yoshioka, and Yoshiyuka Kaneda -- Wenlu Zhu. Section II: the view from the lab The habitat of fault-generated pseudotachylyte: presence vs. absence of friction-melt / Pseudotachylyte-nearing strike-slip faults in mylonitic host rocks, Fort Foster brittle zone, Kittery, Maine / Energentics of chemical alteration in fault zones and its relationship to seismic cycle / How thick is this fault? fault displacement-thickness scaling revisited / Episodic fluid flow in an aseismic overpressured growth fault, northern Gulf of Mexico / Mechanics and interpretations of fault slip / The missing sinks: slip localization in faults, damage zones, and the seismic energy budget / Richard H. Sibson and Virginia G. Toy -- Mark T. Swanson -- Joseph R. Jacobs, James P. Evans, and Peter T. Kolesar -- Zoe K. Shipton, Aisling M. Soden, James D. Kirkpatrick, Aileen M. Bright, and Rebecca J. Lunn -- Steven Losh and Matthew Haney -- Stephen J. Martel and Christin Shacat -- Zoe K. Shipton, James P. Evans, Rachel E. Abercrombie, and Emily E. Brodsky. Section III: the view from the field Seismic radiation from simple models of earthquakes / On the mechanical work absorbed on faults during earthquake ruptures / Properties of dynamic earthquake ruptures with heterogeneous stress drop / The effects of flash-weakening and damage on the evolution of fault strength and temperature / Impact of friction and scale-dependent initial stress on radiated energy-moment scaling / On scaling of fracture energy and stress drop in dynamic rupture models: consequences for near-source ground-motions / Mechanics of sliding in rate/state friction experiments / R. Madariaga, J.-P. Ampuero, and M. Adda-Bedia -- Massimo Cocco, Paul Spudich, and Elisa Tinti -- J.-P. Ampuero, J. Ripperger, and P.M. Mai -- A.W. Rempel -- Bruce E. Shaw -- P.M. Mai, P. Somerville, A. Pitarka, L. Dalguer, S. Song, G. Beroza, H. Miyake, and K. Irikura -- J.B. Walsh. Section IV: earthquakes in theory The strength of the San Andreas Fault: a critical analysis / What do faults feel? observational constraints on the stresses acting on seismogenic faults / Christopher H. Scholz -- John Townend. Section V: How efficient is the "earthquake machine" and how strong are its working parts?
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Seismic waves. Energy dissipation. Faults (Geology) Seismology. Energy dissipation. Faults (Geology) Seismic waves. Seismology.